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High-latitude freeze and thaw states detection using satellite-based microwave land surface emissivity estimates

机译:使用基于卫星的微波陆地表面发射率估算值进行高纬度冻结和解冻状态检测

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Freeze and thaw (FT) processes have profound impact on the terrestrial water cycle, net primary productivity, carbon cycle, surface energy budget and hence the global climate system. The available passive microwave based FT states data are basically developed from brightness temperatures, which themselves affected by atmospheric water vapor content. Since land surface emissivity estimates derived from passive microwave observations are free from atmospheric effects, the use of land emissivity in FT states detection is promising. The objective of this study is to estimate land surface emissivity from the Advanced Microwave Scanning Radiometer-2 observations and to investigate its potential for high-latitude FT states detection. The instantaneous land surface emissivity is computed using an improved algorithm along with near-simultaneous ancillary data sets. The difference of estimated land emissivity between higher and lower frequency channels shows great potential for FT states detection.
机译:冻结和融化(FT)过程对陆地水循环,净初级生产力,碳循环,地表能量收支以及全球气候系统都有深远的影响。可用的基于无源微波的FT状态数据基本上是根据亮度温度开发的,亮度温度本身受大气中水汽含量的影响。由于从被动微波观测获得的地表发射率估计不受大气影响,因此在FT状态检测中使用地表发射率是有希望的。这项研究的目的是根据高级微波扫描辐射计2的观测值来估计陆地表面的发射率,并研究其在高纬度FT状态检测中的潜力。使用改进的算法以及近同时的辅助数据集来计算瞬时陆地表面发射率。较高和较低频率信道之间的估计陆地发射率差异显示了FT状态检测的巨大潜力。

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